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The composite evolution of west and east Atlantic cyclone is likely to be different as they develop in different environmental conditions. • East Atlantic cyclones develop faster than west Atlantic cyclones and have lower mslp, this may be due to the existence of a preexisting parent cyclone in the vicinity of the cyclone. • West Atlantic cyclones have higher low-level PV, this may be generated by friction in the boundary layer or latent heat release. • The ratio of upper-to lower-level qgdoi:10.1175/2008mwr2491.1 fatcat:3joq23nq3jar5mwepuqxcr4jwi